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Introduction to Sports Biomechanics: Analysing Human Movement ...

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The velocity can be obtained from the gradient – or slope – of a displacement–time<br />

graph. Likewise acceleration can be obtained from the slope of a velocity–time<br />

graph if we have one.<br />

The acceleration can be obtained from the curvature of a displacement–time graph.<br />

So, from our displacement–time graph, we can qualitatively describe two further<br />

movement patterns; we can specify important features of the velocity–time pattern and<br />

the acceleration–time pattern. As we will now see, this qualitative information will<br />

answer fully the questions that our hypothetical sprint coach posed above.<br />

The gradient – or slope – of a line should be intuitive. All you need <strong>to</strong> do is <strong>to</strong><br />

consider ‘walking’ along the graph from left <strong>to</strong> right:<br />

If you are going uphill, the gradient, that is the velocity, is positive. This happens<br />

throughout Figure 3.6.<br />

If you are going downhill, the gradient and velocity are negative.<br />

Where the direction changes from uphill <strong>to</strong> downhill, the gradient and velocity are<br />

zero, and the gradient and velocity change from positive <strong>to</strong> negative.<br />

Likewise, where the direction changes from downhill <strong>to</strong> uphill, the gradient and<br />

velocity are zero and the gradient and velocity change from negative <strong>to</strong> positive.<br />

This doesn’t, perhaps, seem <strong>to</strong> help much with our coach’s questions.<br />

Curvature is probably less intuitive, so let us define two types of curvature as in<br />

Figure 3.7, which we can call ‘valley-type’ and ‘hill-type’ curvature; we will also use the<br />

terms ‘positive’ and ‘negative’ curvature. Positive curvature is what you would see<br />

looking at a simple curved valley from the side and negative curvature corresponds<br />

<strong>to</strong> the side view of a simple curved hill (Figure 3.7). Let us walk along the graph in<br />

Figure 3.6 again, seeking this time <strong>to</strong> indicate curvature not gradient. At the start<br />

of the race, the curvature is positive (valley-type); somewhere it changes at about 60%<br />

of the race time <strong>to</strong> negative. And what is the gradient doing there? It changes from<br />

becoming steeper <strong>to</strong> becoming less steep; in other words, the velocity s<strong>to</strong>ps increasing<br />

and starts decreasing (Figure 3.8). Our coach’s novice performer takes 60% of the race<br />

<strong>to</strong> reach maximum speed and then starts <strong>to</strong> slow down; we have answered our coach’s<br />

question. This pattern is not, I must admit, typical for a good sprinter, who would<br />

probably maintain a constant speed from about 30 m <strong>to</strong> 90 m, before slowing slightly,<br />

Figure 3.7 Top: positive (valley-type) curvature; bot<strong>to</strong>m: negative (hill-type) curvature.<br />

MORE ON MOVEMENT PATTERNS – THE GEOMETRY OF MOTION<br />

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